Transcript Slide 1

Meteorology for the Soaring Pilot
Joerg Stieber
Canadian Advanced Soaring
Why do we need to know this?
A profound understanding of the weather is the
basis for reaching your goals as a XC Pilot.
• Macro weather
– Weather systems (Highs, Lows, fronts)
– Rain or shine
• Micro weather
– Why are the cu here and not there?
– Local effects like convergence, lake effect, etc.
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The Atmosphere
• Think of it as an ocean of air
• All weather relevant to gliding occurs
below 35,000ft (Troposphere)
• Different airmasses and their
properties
– Temperature
– Humidity
• Warm air can hold more moisture than cold
air
• Percent of saturation (public weather)
• Dew point: Temperature at which an airmass
is saturated (aviation reports)
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Fronts
• Fronts are boundaries between different
airmasses
• They pass over us as airmasses move like
currents in an ocean
– Cold Front
• Cold air displaces warm air
– Temperature drop, gusty NW winds, likely rain, possibly
thunder, quick passage – clear behind
– Warm Front
• Warm air displaces cold air
– Thickening layers of clouds, steady rain, slow passage
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Cold Front
Good soaring
conditions
Ground
18 – 24 hrs
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Tephi
Warm Front
Ground
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Weather Systems
• Low Pressure System
– Cyclone
– Unstable airmass, rises –
clouds and precipitation
– Inflow counter clock wise
(northern hemisphere)
– Mixing of different
airmasses - fronts
• High Pressure System
– Anticyclone
– Airmass sinks (0.2 kts)
– Clockwise outflow
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Isobars
Weather Maps
www.intellicast.com/National/Surface/Mixed.aspx
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How Thermals Work
• Sun heats the
ground (not the air)
• Ground transfers
heat to the lowest
layers of air
• A pocket of hot air
develops at ground
level
• Eventually the pocket
of hot air takes off
20 C
20 C
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20 C
25 C
9C
15 C
9C
• The parcel of air cools as a result of
expanding as the pressure drops with height
– adiabatic lapse rate – dry / wet
• Environmental lapse rate ~ -2C per 1000ft
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Unstable
15 C
15 C
15 C
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Unstable
17 C
15 C
17 C
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Questions??
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4000
Inversion
Back to
Cold Front
3000
Dry Adiabatic Lapse Rate
2000
1000
Ground
Inversion
0
20
10
Temperature
Tephigram
Trigger 30
The Tephigram
• Temperature and humidity over altitude
• The tephigram shows if a particular airmass
is stable or unstable and allows us to forecast
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–
–
–
–
thermal strength
depth (height) of convection
trigger temperature
Clouds
Overdevelopment
• The easiest to use is the NOAA Java based
plot at: http://rucsoundings.noaa.gov
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Skewed Tephi
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4 Different Tephis
(Dave Springford)
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•
•
•
Blue soaring day
Good soaring day
Over-development
Cu spreading out
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Convection without Clouds
the dreaded blue day
Saturation
point follow
mixing ratio
moisture
content of
parcel
(Dave Springford)
parcel stops
rising before
saturating
parcel rises while unstable
(along dry adiabatic LR)
Ground temp
from daytime
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heating
Convection with Clouds
Fair weather Cu
(Dave Springford)
temperature profile of
airmass includes upper level
inversion
parcel stops rising
clouds between
825 and 875 mb
saturated parcel continues to
rise along wet adiabatic LR
parcel saturates here
moisture content
parcel rises while unstable
along dry adiabatic LR
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Over Development (CBs)
(Dave Springford)
temperature profile of
airmass does not include
inversion until 40,000 ft
clouds
between 825
and < 200 mb
saturated parcel rises
along wet adiabatic LR
parcel saturates
parcel rises
while unstable
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Towering Cu - Precip
Showers are still flyable but one has to keep a close
eye on the weather and pick the route carefully
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CBs – Thunderstorms
Better make sure the plane is secure!
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CBs – Thunderstorms
Better make sure the plane is secure!
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(Dave Springford)
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Questions??
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Looking a Week ahead
Any good Days coming up?
• Long-term forecast (5 – 7 days)
– Public forecast: www.weatheroffice.gc.ca/
– www.theweathernetwork.com/fourteenday/caon0356?ref=qlink_st_14day
– Unisys 10 day forecast: http://weather.unisys.com/
• Forecast maps for days 2-3
Unisys Map
– Intellicast www.intellicast.com/National/Surface/Forecast36.aspx
• Dr. Jack/XC Skies for days 1-2-3 NAM & RUC
– http://www.drjack.info/BLIP/index.html
Dr Jack
Jump to Day
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(Dave Springford)
Good Weather Systems
Back to Week ahead
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SW
Ontario
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On the Day of the Flight
• Look out the window
– You should see clear blue sky or small low cu (after a recent cold front)
– The air should feel fresh and cool
• Public forecast
– WX, max temperature, dew point, any change later?
– Cloud base in ft AGL = 400*(Tmax – Tdewp) (if the thermals go that high)
• Tephi for Kitchener/London (16z, 18z, 21z)
– Airmass, height of inversion, cu?, winds aloft
• Satellite Picture – clear?
• Nav Canada – Prog Charts (18z)
– change in airmass expected?
• Dr. Jack or XC-Skies
– thermal strength, height, cu, boyancy/shear (18z, 21z)
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Special Situations
• Cloud streets
Cloud Street
– On windy days – form upwind/downwind
• Lake effect
– Wind off the lakes
• L. Ontario (E-wind), Erie (S-wind), Huron NW
• Sea breeze
Lake Effect
– General wind direction 5 – 10 kts off-shore
• Convergence
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Convergence
Cloud Street
Back
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Back
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Lake Effect due to
easterly wind
Lake Effect & Convergence
Seabreeze along Lake Huron
Convergence on the Niagara Peninsula
Convergence West of London
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Internet Sources
(Dave Springford)
• The first thing you need is a public forecast from Environment
Canada to give a general weather picture
– Sun or rain?
– Max temp for the day?
– Wind direction?
For what Period?
Dewpoint?
• Next an overall picture of the frontal systems in NA is helpful
– I use either Intellicast or Unisys
• A satellite picture can also help
– the GOES Satellite picture is good: http://weather.unisys.com/satellite/
– Weatherundergound:
(check the IR too)
http://www.wunderground.com/satellite/vis/1k/US.html
• A clouds and weather forecast from NavCanada is also helpful